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dc.contributor.authorAbdel Gawad, A. E.en
dc.contributor.authorAli, K. G.en
dc.contributor.authorWahed, A. A. A.en
dc.contributor.authorAlsafi, K.en
dc.contributor.authorKhafaji, M.en
dc.contributor.authorAlbahiti, S.en
dc.contributor.authorKhalil, M.en
dc.contributor.authorMasoud, M. S.en
dc.contributor.authorHanfi, M. Y.en
dc.date.accessioned2022-10-19T05:20:32Z-
dc.date.available2022-10-19T05:20:32Z-
dc.date.issued2022-
dc.identifier.citationExcess Lifetime Cancer Risk Associated with Granite Bearing Radioactive Minerals and Valuable Metals, Monqul Area, North Eastern Desert, Egypt / A. E. Abdel Gawad, K. G. Ali, A. A. A. Wahed et al. // Materials. — 2022. — Vol. 15. — Iss. 12. — 4307.en
dc.identifier.otherhttps://www.scopus.com/inward/record.uri?eid=2-s2.0-85132800246&doi=10.3390%2fma15124307&partnerID=40&md5=587f6060584aeee320e7ed32859e8f9blink
dc.identifier.urihttp://elar.urfu.ru/handle/10995/117934-
dc.description.abstractThe present work is concerned with assessing the cancer risk contributed by the studied granite types including valuable metals, such as Cu, Au, and Ba mineralization, as well as radioactive-bearing mineralization, such as monazite and zircon, in south Monqul at Wadi Makhrag El Ebel, north Eastern Desert, Egypt. The mineralization analyses illustrated that copper mineralization containing chrysocolla and tenorite minerals were restricted to the alteration zone, especially (argillic, phyllic, and propylitic) in monzogranite. However, barite veinlets had an ENE–WSW trend, while gold mineralization was confined to quartz veins having NE–SW trends. Monazite and zircon are radioactive-bearing minerals recorded in monzogranite causing high radioactive zones in south Monqul. The radionuclide activity concentrations were detected in the studied monzogranites. The mean values of AU (103 ± 91 Bq kg−1), ATh (78 ± 19 Bq kg−1), and AK (1484 ± 334 Bq kg−1) in the monzogranite samples were higher than the recommended worldwide average. The change in radioactive-transporting minerals found inside granite faults caused the high amounts of radioactivity seen in the samples. Due to the monzogranites being applied in building materials, the radiological hazards were assessed by calculating risk indices such as annual effective dose (AED) and excess lifetime cancer risk (ELCR). The acceptable limit for the ELCR readings was surpassed. As a result, the investigated monzogranite samples are not suitable for use in infrastructure materials. © 2022 by the authors. Licensee MDPI, Basel, Switzerland.en
dc.format.mimetypeapplication/pdfen
dc.language.isoenen
dc.rightsinfo:eu-repo/semantics/openAccessen
dc.sourceMaterialsen
dc.subjectHAZARD EFFECTSen
dc.subjectMONZOGRANITESen
dc.subjectRADIOACTIVE-BEARING MINERALSen
dc.subjectRADIOACTIVITYen
dc.subjectSPECTROSCOPYen
dc.subjectVALUABLE METALSen
dc.subjectDISEASESen
dc.subjectHAZARDSen
dc.subjectMINERALOGYen
dc.subjectPHOSPHATE MINERALSen
dc.subjectRADIATIONen
dc.subjectRADIOACTIVITYen
dc.subjectRISK ASSESSMENTen
dc.subjectZIRCONen
dc.subjectALTERATION ZONESen
dc.subjectCANCER RISKen
dc.subjectCHRYSOCOLLAen
dc.subjectCOPPER MINERALIZATIONen
dc.subjectGOLD MINERALIZATIONen
dc.subjectHAZARD EFFECTen
dc.subjectMINERALISATIONen
dc.subjectMONZOGRANITEen
dc.subjectRADIOACTIVE-BEARING MINERALen
dc.subjectVALUABLE METALSen
dc.subjectGRANITEen
dc.titleExcess Lifetime Cancer Risk Associated with Granite Bearing Radioactive Minerals and Valuable Metals, Monqul Area, North Eastern Desert, Egypten
dc.typeArticleen
dc.typeinfo:eu-repo/semantics/articleen
dc.typeinfo:eu-repo/semantics/publishedVersionen
dc.identifier.doi10.3390/ma15124307-
dc.identifier.scopus85132800246-
local.contributor.employeeAbdel Gawad, A.E., Nuclear Materials Authority, P.O. Box 530, El-Maadi, Cairo, 11728, Egypten
local.contributor.employeeAli, K.G., Nuclear Materials Authority, P.O. Box 530, El-Maadi, Cairo, 11728, Egypten
local.contributor.employeeWahed, A.A.A., Nuclear Materials Authority, P.O. Box 530, El-Maadi, Cairo, 11728, Egypten
local.contributor.employeeAlsafi, K., Medical Physics Unit, Department of Radiology, Faculty of Medicine, King Abdulaziz University (KAU), Jeddah, 22252, Saudi Arabia, Medical Physics Unit, Diagnostic Imaging Department, King Abdulaziz University Hospital, Jeddah, 22252, Saudi Arabiaen
local.contributor.employeeKhafaji, M., Medical Physics Unit, Department of Radiology, Faculty of Medicine, King Abdulaziz University (KAU), Jeddah, 22252, Saudi Arabia, Medical Physics Unit, Diagnostic Imaging Department, King Abdulaziz University Hospital, Jeddah, 22252, Saudi Arabiaen
local.contributor.employeeAlbahiti, S., Medical Physics Unit, Department of Radiology, Faculty of Medicine, King Abdulaziz University (KAU), Jeddah, 22252, Saudi Arabia, Medical Physics Unit, Diagnostic Imaging Department, King Abdulaziz University Hospital, Jeddah, 22252, Saudi Arabiaen
local.contributor.employeeKhalil, M., Geology Department, Faculty of Science, Damietta University, Damietta, 34511, Egypten
local.contributor.employeeMasoud, M.S., Nuclear Materials Authority, P.O. Box 530, El-Maadi, Cairo, 11728, Egypten
local.contributor.employeeHanfi, M.Y., Nuclear Materials Authority, P.O. Box 530, El-Maadi, Cairo, 11728, Egypt, Institute of Physics and Technology, Ural Federal University, Ekaterinburg, 620002, Russian Federationen
local.issue12-
local.volume15-
dc.identifier.wos000816401500001-
local.contributor.departmentNuclear Materials Authority, P.O. Box 530, El-Maadi, Cairo, 11728, Egypten
local.contributor.departmentMedical Physics Unit, Department of Radiology, Faculty of Medicine, King Abdulaziz University (KAU), Jeddah, 22252, Saudi Arabiaen
local.contributor.departmentMedical Physics Unit, Diagnostic Imaging Department, King Abdulaziz University Hospital, Jeddah, 22252, Saudi Arabiaen
local.contributor.departmentGeology Department, Faculty of Science, Damietta University, Damietta, 34511, Egypten
local.contributor.departmentInstitute of Physics and Technology, Ural Federal University, Ekaterinburg, 620002, Russian Federationen
local.identifier.pure30543448-
local.description.order4307-
local.identifier.eid2-s2.0-85132800246-
local.identifier.wosWOS:000816401500001-
local.identifier.pmid19961944-
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